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Mojave River Valley Museum
Death Valley Geology
Basin & Range Province
The Rise and Fall of Death Valley's Mountain Ranges and valleys
Dante's View provides a spectacular look at Death Valley's remarkable scenery. From this vantage point you
can view distant 11049 ft. Telescope Peak to Badwater, the lowest point (-282 ft.) in the Western Hemisphere. This
difference in elevation is a staggering 11,331 feet (3455 m) — the greatest topographic relief in the conterminous
U.S.. This striking
is a product of Death Valley's very active tectonics.
Stretched to the Breaking Point
The forces that created this distinctive topography begin deep beneath the Earth's surface. Tension created by movements of Earth's tectonic plates have stretched the rocky crust Basin and Range province to the breaking point. The entire region has been pulled apart, fracturing the crust and creating large faults. Along these roughly north-south-trending faults mountains have uplifted and valleys down-dropped, producing the distinctive alternating pattern of linear mountain ranges and valleys of the Basin and Range province. Dante's View is a perfect place to see the results of Death Valley's very active fault system. The steep mountain face on which you are standing rose up along the fault while the valley floor descended. The deep Death Valley basin is filled with sediments eroded from the surrounding mountains.
Dante's View - Death Valley Regional Geology
Dante’s view is one of four relatively accessible high points that offer truly amazing views of Death Valley (see also Sites GF1, NP6 and CM3). Of the four, Dante’s view is the most accessible and most popular. ...
Physiography - Mountains & Basins
The Mojave Desert region is within a great inland (isolated) drainage basin. Not for perhaps 10 million years ...
Striking topography; 11049 ft. Telescope Peak to Badwater, the lowest point (-282 ft.) in the Western Hemisphere. This difference in elevation is a staggering 11,331 feet (3455 m) — the greatest topographic relief in the conterminous U.S.
The deep Death Valley basin is filled with sediment eroded from the surrounding mountains.
The western face of Dante's peak shows the abrupt result of Death Valley's tectonics.